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  • 7/28/2019 Catalogue SV

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  • 7/28/2019 Catalogue SV

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    The following features are common to all our finite elemepackages:

    Simulation FeaturesuFully automatic mesh generation. Mesh generation may be

    by a maximum number of nodes or by a maximum specifieuFully automatic mesh refinement. Mesh refinement is base

    relative error of the governing equation and therefore autolocates critical zones. In a transient analysis a different mesgenerated for each time step. Our packages are currently tpackages in the world to offer this feature applied to geoteengineering.u

    Finite element analysis by the Galerkin method. The solveradvanced features such as preconditioning of the convergematrix as well as staging and automatic mesh refinement tsolutions with greater stability than any other software curavailable.uFully automatic time-step refinement for transient analysis

    steps selected by the solver are independant of the plottinselected by the user.

    Model Design FeaturesuCAD style view entry of geometry and other modeling objeu3D models built as stacked surfaces. Each surface may be i

    from Surfer or any XYZ data text fil e.uEach surface may have multiple regions defined.uSurface grids are independant of region geometry and ma

    irregular or overlap.uImport AutoCAD .dxf geometry and incorporate it directly

    model. The automatic mesh generation will automatically apoints with line segment end points.uGraphical model design may be exported as a WMF or DXF

    printed.uBitmap or DXF geometry may be imported and layered be

    geometry to simplify model creation (version 3.0).

    Output Features without TecPlot ModuleuColor 2D contour plots of all solution variables may be prod

    any X, Y, or Z plane section through the problem.uPlots may be zoomed to i solate any region of interest.u2D Vector plots of any component variable may be produc

    X, Y, or Z plane section through the problem.uVolume or mass integrals may be computed over the entire

    or any particular region of interest.uMesh plots track general mesh refinement.uPlots of value versus time may be generated at any coordin

    solution variable.uGraphical output may be exported to BMP or PNG formats

    Output Features with TecPlot ModuleuColor visualization of 3D mesh is available.uTransparency allows visualization of internal mesh and/or uCutaways allow user to view internal sections of the modeuColor 3D contour plots of any solution variable may be plac

    face of the model. Custom color shadings may be specifieduIsosurfaces may be plotted.

    uOverlaying of plots may be performed. For example, vectorshown in Region 1 while contours of head may be shown iu3D Vector plots of gradients.uText and line art may be added to output.uGraphical output may be exported to WMF, DXF, JPG, or BMuPlotting of 3D streamtraces.uAnimation of 2D or 3D transient results.uOverlay of DXF files.

    oftware Features

    SVDynamic 2D

    SoilVision Database

    SVFlux 2D / 3D

    ChemFlux 2D / 3D

    mulation FeaturesSteady-state or transient (time-dependant) analysis.Saturated or unsaturated analysis.Flux sections may be placed on internal or external irregular surfacesand/or extruded walls of the problem. Water flow with time may betracked across flux sections.Anisotropic analysis at any angle (version 3.0). 3D anisotropy isdefined by two angles.Add contaminant transport analysis with our ChemFlux software.

    odel Design FeaturesHead or flux boundary conditions may be specified as contants or

    free-form equations. Free form equations may be specifi ed as afunction of position or time (i.e., h=30+exp(t)*2.5)Tables of net flux data may be cut and pasted into SVFlux to act asboundary conditions. This feature allows modeling of flux boundarieswhere weather station data is available. The z component of verticalflux boundaries may be isolated to simulate precipitation on steeprregular surfaces.mport soil-water characteristic curve or permeability data from the

    SoilVision software. The SoilVision database contains laboratory dataon over 6000 soil -water characteristic curves, over 2500 ksat values,and over 400 unsaturated permeability curves.nitial water table for a transient analysis may be entered as a surface

    or imported as heads from a steady-state analysis.

    pplicationsUnconfined flow.nfiltration / precipitation.

    Design of earth covers.Pond infiltration.Excess pore-water pressure build-up and dissipation.Seepage modeling involving geomembranes.Water and contaminant movement (with ChemFlux) in mine tailings

    and leach pads.Time-dependant water flow.Water (and contaminant) flow in the unsaturated (vadose) zone.Aquifer recharge.Dam seepage.

    stem Requirements (All Packages)nite Element 2D/3D packages run on Windows 95/98, NT 4.0, Me, 2000,d XP. The recommended minimum hardware configuration is a P266th 128MB RAM and 35 MB hard disk space.

    mulation FeaturesTransient (time dependant) analysis.Saturated or unsaturated analysis.Model advection, diffusion, adsorption, and radioactive orbiological decay.mport groundwater gradients from SVFlux.

    Flux sections may be placed on internal or external irregularsurfaces and/or extruded walls of the problem.Contaminant flow with time may be tracked a cross flux sections.Fully automatic mesh generation and refinement. Mesh refinements based on the relative error of the governing equation and

    therefore automatically locates critical zones. In a transient analysisa different mesh is generated for each time step. Mesh refinementallows reduction in numerical dispersion and artificial oscillationnumerical problems typically encountered in contaminanttransport models. ChemFlux is currently the only groundwaterpackage in the world to offer mesh refinement.

    Mesh refinement can be set to follow the contaminant frontwhereby greatly increasing solution stability and accuracy.Fully automatic time-step refinement for transient a nalysis. Thetime-steps selected by the solver are independant o f the plottingntervals selected by the user.

    odel Design Featuresmport geometry from SVFlux.

    Concentration or flux boundary conditions may be specified ascontants or free-form equations. Free form equations may bespecified as a function o f position or time (i.e. C=0.8+exp(t)*0.3).

    pplicationsSingle-phase miscible contaminant movement.Movement of contaminants out of tailings pits a nd earthcontainment facilities.Solution of advection-dominated problems typically plagued byconvergence problems.Modeling of problems dominated by radioactive or biologicaldecay.Model contaminant movement through any combination of

    advection, dispersion, adsorption and/or decay.

    SVHeat 2D / 3D

    SVSolid 2D / 3D

    Simulation FeaturesuSteady-state analysis.uTransient (time dependant) analysis.uSaturated or unsaturated analysis.uFlux sections may be placed on internal or external irregular

    surfaces and/or extruded walls of the problem.uEnergy with time may be tracked across flux sections.uFully automatic time-step refinement for transient a nalysis. The

    time-steps selected by the solver are independant o f the plottingintervals selected by the user.uSVHeat is designed to model the transition between frozen and

    unfrozen soils. Functional properties such as thermal conductivity

    versus temperature and unfrozen water content versustemperature may be entered to describe the phase changerelationship between ice and water. Specific heat may be specifiedto follow the constant or Newman formulation.

    Model Design FeaturesuHead or flux boundary conditions may be specified as contants or

    free-form equations. Free form equations may be specified as afunction of position or time (i.e., T=30+exp(time)*2.5+0.5*y).uInitial water contents may be imported from a SVFlux analysis.

    ApplicationsuThermal design of roads and airstrips.uGround freezing for soil stabilization.uInsulation design for shallow buried piping.uThawing beneath heated or chilled structures.uFreezing around chilled pipelines.uTemperature variation over large areas with significant relief.

    Simulation Features

    SVDynamic represents a revolutionary new method of slope stabilityanalysis that extends the capabilities of limit equilibrium methods ofanalysis.

    Slope stability analysis is an integral part of many geotechnicalengineering studies. Although numberous methods of analysis exist,the failure mechanism is still not fully understood.

    Force and moment equilibrium methods can be ap plied to thestability problem and will provide a computed factor of safety. Alllimit equilibrium methods rely on a critical assumption regarding theshape of the slip surface. The normal force on the base of the slice isdetermined by applying statistical equilibrium to a slice from thesliding mass. The location of the critical sli p surface is determined bytrial and error.

    SVDynamic makes use of a finite element stress analysis (SVSolid) tocompute the stress state in a soil mass. Various soil models can beused for the computation of the stress states. SVDynamic makes useof dynamic programming to calculate the most probable location of

    the slip surface. No assumption needs to be made regarding theshape of the slip surface since the determination of the shape is partof the solution. Non-circular slip surfaces may be computed fromirregular soil layering.

    The SVDynamic solution provides a global factor of safety as well asthe distribution of the local factors of safety along the critical slipsurface.

    DescriptionSoilVision is the premiere product worldwide for the estimatiunsaturated soil properties. The knowledge-based componeprovide input for analysis of unsaturated soils. SoilVision prov20 journal published algorithms for the estimation of soil prorequired for unsaturated seepage modeling. A soils databaselaboratory data on over 6000 soils is also included. SoilVisionthe modeler in estimating suitable input for the modeling ofunsaturated soil processes independent of extensive laboratoprograms.Key FeaturesuOver 20 journal published estimation methods - estimate u

    soil properties for seepage modeling.uMathematical fitting of soil functions.uProfessional reporting.

    Advantages over other solutionsuTheoretical estimation of soil propertiesuPre-existing laboratory database of over 6000 soilsuGeostatistics module allows quick statistical analysis of you

    laboratory datauOnly commercial database application in the world capable

    managing unsaturated soils information.uManagement of geoenvironmental data.uAutomatic soil texture classification by the USDA or USCS (A

    methods.uMathematical fits of soil property functions allows soils in c

    "bands" to be selected.u

    Mathematical model provides input for finite element and difference models.

    Simulation FeaturesuFive different soil models including linear ela stic, Duncan and

    Chang, as well as a nonlinear model.uSoil models may vary by region. For example, a soil using a linear

    elastic model may be adjacent to a soil using the Duncan andChang model.uUnsaturated deformations of soils may be modeled.uInitial conditions may be impor ted from a previous analysis. The

    OCR of a previous analysis may be specified to determine the initial

    preconsolidation pressure of the current analysis. Any variable froma previous analysis may be specified as an initial condition for thenext analysis.uAnisotropic analysis at any angle in 2D or 3D.uAxisymmetric analysis.uUse of Skempton's A and B parameters to compute pore-water

    pressure build-up.

    Model Design FeaturesuFree, fixed, displacement constant or expression, force contant or

    expression, or water boundary conditions may be specified. Freeform equations may be specified as a function of position (i.e.d=0.5+log(x)*0.1).uInitial water table may be graphically drawn on the problem or

    imported from an SVFlux analysis.

    ApplicationsuFoundation design.uRegional subsidence due to pumping of aquifers.uDesign of slab foundations subjected to unsaturated shrinking or

    swelling.uEmbankment or excavation construction.

    uSmall-strain consolidation analysis when coupled with SVFlux.uExcess pore-water pressures caused by the placement of fill.uModeling of problems with complex geometry.

    w.soilvision.com p 1.306.477.3324 p [email protected] p fax 1.306.955.4575

    Common Features